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首页> 外文期刊>River Research and Applications >Fragmentation of an Intermittent Stream During Seasonal Drought: Intra-annual and Interannual Patterns and Biological Consequences
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Fragmentation of an Intermittent Stream During Seasonal Drought: Intra-annual and Interannual Patterns and Biological Consequences

机译:季节性干旱期间间歇性河流的破碎:年内和年际模式与生物后果

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Intermittent streams lose surface flow during some portion of the year and can be important breeding and rearing habitats for stream biota. However, habitat contraction and deteriorating water quality across the summer can result in harsh conditions and mortality. We explored patterns of drying in a small intermittent stream across the summer in Mediterranean-climate California, including across 4years that differed in antecedent precipitation. Wet-dry mapping revealed earlier stream fragmentation following dry winters and that entire sections of the stream varied in their propensity to dry suggesting an important influence of geomorphology on drying. Within two slow-drying' reaches, initial riffle volumes were higher following wetter winters, but the rate of riffle drying was higher following wet years, presumably because higher initial volumes resulted in greater drying capacity. Initial pool volumes were similar across years, but the rate of pool drying was faster following dry versus wet winters (pool half-life ranged from 9.7weeks in the driest year to 26.3weeks in the wettest year). Stream temperature differed among years, but differences were slight, and temperatures rarely exceeded optimal conditions for trout growth. We observed limited movement of trout during drier years and found that movement was negatively associated with pool depth, riffle length and date, and positively associated with riffle volume. Overall, we found that antecedent rainfall influenced variability in pool drying more than riffle drying, that entire sections of the creek varied in their propensity to dry and that biological fragmentation preceded physical fragmentation by 3 to 7weeks. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:间歇性溪流在一年中的某些时间段会损失地表水,可能是重要的繁殖和养殖溪流生物的栖息地。但是,整个夏天的栖息地收缩和水质恶化可能导致恶劣的条件和死亡。我们探索了整个夏季在地中海气候加州的一小段间歇性干流中的干燥方式,包括四年间不同的前期降水。湿干测绘揭示了冬季干燥后河流的早期破碎,整个河段的干燥倾向各不相同,这表明地貌对干燥有重要影响。在两个缓慢干燥的范围内,冬季较湿后初始浅滩的体积较高,但湿年后浅滩的干燥速率较高,这大概是因为较高的初始体积导致了更大的干燥能力。多年来,初始池数量相似,但是与干燥冬季相比,干燥冬天池的干燥速度更快(池半衰期从最干燥的一年的9.7周到最潮湿的一年的26.3周不等)。溪流温度在几年间有所不同,但差异很小,温度很少超过鳟鱼生长的最佳条件。在较干燥的年份,我们观察到鳟鱼运动受限,发现运动与池深度,鱼鳞长度和日期呈负相关,与鱼鳞体积呈正相关。总的来说,我们发现,前期降雨对水池干燥的可变性影响比对浅滩干燥的影响更大,小溪的整个断面的干燥倾向均发生变化,并且生物破碎先于物理破碎3至7周。版权所有(c)2015 John Wiley&Sons,Ltd.

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